Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis

Seismicity in the Eastern Baltic Sea region is lower than in the Fennoscandian shield. High seismicity of the shield in the last 13 000 years is well reflected in the Quaternary deposits. So far, no evidences of seismites have been described in the studies of the territory. Recent analysis of the Qu...

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Main Authors: Bitinas, Alfredas, Lazauskienė, Jurga
Format: Article in Journal/Newspaper
Language:Lithuanian
English
Published: 2011
Subjects:
Online Access:http://vu.lvb.lt/VU:ELABAPDB4489696&prefLang=en_US
id ftlitinstagrecon:oai:elaba:4489696
record_format openpolar
spelling ftlitinstagrecon:oai:elaba:4489696 2023-05-15T16:12:56+02:00 Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis Implications of the palaeoseismic events based on the analysis of the structures of the Quaternary deposits Bitinas, Alfredas Lazauskienė, Jurga 2011 http://vu.lvb.lt/VU:ELABAPDB4489696&prefLang=en_US lit eng lit eng http://vu.lvb.lt/VU:ELABAPDB4489696&prefLang=en_US Baltica, Vilnius : Lietuvos geografų draugija, 2011, vol. 24, special issue, p. 127-130 ISSN 0067-3064 seismicity paleosesmic events seismites Quaternary deposits Eastern Baltic sea region info:eu-repo/semantics/article 2011 ftlitinstagrecon 2021-12-02T01:31:13Z Seismicity in the Eastern Baltic Sea region is lower than in the Fennoscandian shield. High seismicity of the shield in the last 13 000 years is well reflected in the Quaternary deposits. So far, no evidences of seismites have been described in the studies of the territory. Recent analysis of the Quaternary deposits shows that the structures earlier interpreted as cryoturbations, glaciotectonic or water-escape features show characteristics of the liquefaction-inducted deformations. The majority of them are related to the Late Glacial and Holocene and some to Middle Pleistocene, Eemian and Early Weichselian. Article in Journal/Newspaper Fennoscandian LAEI VL (Lithuanian Institute of Agrarian Economics Virtual Library)
institution Open Polar
collection LAEI VL (Lithuanian Institute of Agrarian Economics Virtual Library)
op_collection_id ftlitinstagrecon
language Lithuanian
English
topic seismicity
paleosesmic events
seismites
Quaternary deposits
Eastern Baltic sea region
spellingShingle seismicity
paleosesmic events
seismites
Quaternary deposits
Eastern Baltic sea region
Bitinas, Alfredas
Lazauskienė, Jurga
Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
topic_facet seismicity
paleosesmic events
seismites
Quaternary deposits
Eastern Baltic sea region
description Seismicity in the Eastern Baltic Sea region is lower than in the Fennoscandian shield. High seismicity of the shield in the last 13 000 years is well reflected in the Quaternary deposits. So far, no evidences of seismites have been described in the studies of the territory. Recent analysis of the Quaternary deposits shows that the structures earlier interpreted as cryoturbations, glaciotectonic or water-escape features show characteristics of the liquefaction-inducted deformations. The majority of them are related to the Late Glacial and Holocene and some to Middle Pleistocene, Eemian and Early Weichselian.
format Article in Journal/Newspaper
author Bitinas, Alfredas
Lazauskienė, Jurga
author_facet Bitinas, Alfredas
Lazauskienė, Jurga
author_sort Bitinas, Alfredas
title Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
title_short Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
title_full Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
title_fullStr Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
title_full_unstemmed Paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
title_sort paleoseisminių įvykių prielaidos kvartero nuosėdų tekstūrų tyrimo duomenimis
publishDate 2011
url http://vu.lvb.lt/VU:ELABAPDB4489696&prefLang=en_US
genre Fennoscandian
genre_facet Fennoscandian
op_source Baltica, Vilnius : Lietuvos geografų draugija, 2011, vol. 24, special issue, p. 127-130
ISSN 0067-3064
op_relation http://vu.lvb.lt/VU:ELABAPDB4489696&prefLang=en_US
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